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	<journal>
		<journal_title>Biogeosciences Discussions</journal_title>
		<journal_url>www.biogeosciences-discuss.net</journal_url>
		<issn>1810-6277</issn>
		<eissn>1810-6285</eissn>
		<volume_number>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/bgd-7-25-2010</doi>
	<article_url>http://www.biogeosciences-discuss.net/7/25/2010/</article_url>
	<abstract_html>http://www.biogeosciences-discuss.net/7/25/2010/bgd-7-25-2010.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences-discuss.net/7/25/2010/bgd-7-25-2010.pdf</fulltext_pdf>
	<start_page>25</start_page>
	<end_page>53</end_page>
	<publication_date>2010-01-05</publication_date>
	<article_title content_type="html">The Arabian Sea as a high-nutrient, low-chlorophyll region during the late Southwest Monsoon</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. W. A. Naqvi</name>
			<email>naqvi@nio.org</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. W. Moffett</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. U. Gauns</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. V. Narvekar</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>A. K. Pratihary</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>H. Naik</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>D. M. Shenoy</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>D. A. Jayakumar</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>T. J. Goepfert</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>P. K. Patra</name>
		</author>
		<author numeration="11" affiliations="6">
			<name>A. Al-Azri</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>S. I. Ahmed</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Institute of Oceanography (Council of Scientific &amp; Industrial Research), Dona Paula, Goa 403 004, India</affiliation>
		<affiliation numeration="2" content_type="html">Department of Biological Sciences, University of Southern California, Los Angeles, CA 90089, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Geosciences, Princeton University, Princeton, NJ 08544, USA</affiliation>
		<affiliation numeration="4" content_type="html">Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA</affiliation>
		<affiliation numeration="5" content_type="html">Frontier Research Center for Global Change, JAMSTEC, Yokohama 236 001, Japan</affiliation>
		<affiliation numeration="6" content_type="html">Department of Marine Science and Fisheries, College of Agricultural and Marine Sciences, Sultan Qaboos University, Al-Khod 123, Sultanate of Oman</affiliation>
	</affiliations>
	<abstract content_type="html">Extensive observations during the late Southwest Monsoon of 2004 over the
Indian and Omani shelves, and along an east-west transect reveal a mosaic of
biogeochemical provinces including an unexpected high-nutrient,
low-chlorophyll condition off the southern Omani coast. This feature,
coupled with other characteristics of the system, suggest a close similarity
between the Omani upwelling system and the Peruvian and California upwelling
systems, where primary production (PP) is limited by iron. An
intensification of upwelling, reported to have been caused by the decline in
the winter/spring Eurasian snow cover since 1997, is not supported by in
situ hydrographic and chlorophyll measurements as well as a reanalysis of
ocean colour data extending to 2009. Iron limitation of PP may complicate
simple relationship between upwelling and PP assumed by previous workers,
and contribute to the anomalous offshore occurrence of the most severe
oxygen (O&lt;sub&gt;2&lt;/sub&gt;) depletion in the region. Over the Indian shelf, affected by
very shallow O&lt;sub&gt;2&lt;/sub&gt;-deficient zone, high PP is restricted to a thin,
oxygenated surface layer probably due to unsuitability of the
O&lt;sub&gt;2&lt;/sub&gt;-depleted environment for the growth of oxygenic photosynthesizers.</abstract>
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